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184 MOLLUSCA FROM MIOCENE AND LOWER PLIOCENE OF VIRGINIA AND NORTH CAROLINA<br />

but inconspicuous sutures. Nuclear whorls wanting.<br />

Each of remaining turns sculptured with 4 approximately<br />

equisized and equispaced spirals, very low,<br />

broad, and straplike, mounted with close-set, squarish<br />

tubercles, about 2 to each linear millimeter on the body<br />

whorl; the foundation bands on the earlier whorls<br />

almost or altogether obsolete, the tubercles sharper and<br />

more rounded, thus lending a beaded aspect to the<br />

sculpture of the posterior portion of the shell; a simple<br />

secondary introduced on the penultima at the medial<br />

line of the whorl, midway between the second and third<br />

primaries, later becoming wavy and inconspicuously<br />

beaded. Peripheral keel angular but not sharp, outlined<br />

by a broad, simple, spiral band. Base flattened,<br />

sculptured by strong, slightly rounded spirals varying<br />

somewhat in width and spacing, tending to become<br />

stronger and more distant in the umbilical region; interspaces<br />

sculptured with radiating incrementals.<br />

Aperture badly broken, probably angular, broader than<br />

it is high. Pillar smooth, concave, strengthened by<br />

the reflected callus. Umbilicus imperforate.<br />

The species, though described from a unique type,<br />

is sharply separated from all other forms of this<br />

area by the monotonous pyramidal outline, unbroken<br />

by any angula-rities or convexities of the whorls and<br />

by the 4 rather than 3 primary spirals upon the adolescents<br />

and the squarish tubercles which adorn the adult<br />

spirals. Among the Recent species, its nearest kin is<br />

perhaps Oalliostoma apicinwm Dall of the West Indian<br />

fauna, a slightly smaller, more elevated conch with a<br />

much finer, sharper sculpturing.<br />

Dimensions of holotype: Height 11.1 mm., maximum<br />

diameter 10.0 mm.<br />

Holotype: U.S.N.M. 325470.<br />

Type locality: Eight to 9 miles southeast of Greenville,<br />

Pitt County, N. C. Yorktown formation, zone 2.<br />

In the Oalliostoma philanthropum group, including<br />

the subspecies pontoni Mansfield (pl. 26, fig. 15) and 0.<br />

basicwm Dall (pl. 26, fig. 11), a guide fossil of zone 2<br />

of the Yorktown formation in Virginia and North<br />

Carolina, 0. mitchelli (Conrad) (pl. 26, figs. 19, 23), and<br />

0. ruffinii (H. C. Lea) (pl. 26, fig. 18), the posterior<br />

suture is overhung by the beaded peripheral keel of the<br />

preceding whorl. The group is further removed from<br />

0. cheopsi by the 3 primary spirals on the early whorls<br />

and by the sharp well-rounded beads of the adult ornamentation.<br />

Distribution: Yorktown formation, 8 to 9 miles southeast of<br />

Greenville, Pitt County, N. C.<br />

Calliostoma carolinense Gardner, n. sp.<br />

Plate 26, figures 3, 4<br />

Shell heavy, moderately low; the regularity of the<br />

pyramidal outline broken by the strong spiral cording.<br />

Whorls narrowly tabulated, 6 in number, including the<br />

protoconch, which is very small, probably of not more<br />

than one turn, and, in its decorticated condition, not<br />

readily differentiated from the conch. Initial sculpture<br />

on the conch of 3 spiral lirae, equal in size and<br />

spacing; a fourth spiral introduced on the next to the<br />

last whorl of the spire between the posterior and medial<br />

lirae, increasing somewhat in strength and persistent<br />

but not attaining the prominence of the original primaries;<br />

no other lirae intercalated: on adult whorls<br />

original posterior primary outlining the shoulder; the<br />

anterior, together with the stronger .outer basal spiral,<br />

forming the double peripheral keel; and the medial<br />

of the 3 original spirals, together with a fourth, symmetrically<br />

disposed between the peripheral and shoulder<br />

spirals. Base flattened, heavily sculptured with 4<br />

additional broad straplike cords extending far within<br />

the aperture, separated by interspaces of approximately<br />

their own width; umbilical keel outlined by a similar<br />

spiral. Incremental sculpture microscopically fine.<br />

Suture distinct but not conspicuous, following the anterior<br />

of the peripheral cords, which is commonly partially<br />

visible as a thin, sharp thread directly behind the<br />

suture.<br />

Aperture transversely ovate. ·Outer margin imperfect,<br />

crenulated by the strong spirals. Parietal wall<br />

thinly glazed. Columellar margin concave, simple, reflected.<br />

Umbilical region excavated but not perforate.<br />

Dimensions of holotype: Height 9.8 mm., maximum<br />

diameter 11.2 mm.<br />

Holotype: U.S.N.M. 325472.<br />

Type locality: Hamilton Bluff on the Roanoke River,<br />

Martin County, N.C. Yorktown formation, zone 2.<br />

0 alliostoma carolinense is characterized by the prominence<br />

of the primaries and the reduced number ·of the<br />

secondaries. It is, apparently, an end member of the<br />

0. virginicwm group.<br />

Oalliostoma harrisianrum Olsson, 1916, seems from the<br />

description and the rather poor illustration to be intermediate<br />

between 0. carolinense and 0. virginicum<br />

s. s. In 0. carolinense the regularity of the profile is<br />

broken by the heavy spirals, but the profile of 0. harrisianum<br />

more closely resembles that of 0. virginicum.<br />

The number of spirals is more reduced in 0. carolinense<br />

than it is in either of the two species from Virginia and,<br />

with the possible exception of the peripheral spirals,<br />

they seem to be stronger than those of 0. harrisia1'1ffJJm.<br />

The North Atlantic species Oalliostoma occidentale<br />

Mighels and Adams, 1842, is similar in general aspect,<br />

but the 3 primary spirals are beaded on the juvenile<br />

shells, and the sculpture on the base of the adult is irregular<br />

and tends to become obsolete except toward the<br />

periphery and the umbilical area.<br />

Distribution: Yorktown formation, Hamilton Bluff on the<br />

Roanoke River, Martin County, N. C.

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